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The current methodology for savanna burring only considers the first type of ACCUs (in this case, reducing CH4 and N2O emissions from soils) and does not consider the second type (in this case, soil and biomass carbon sequestration activities).
In any case, soil pH was lower on the older EGRs (8 12 years old at time of survey; installed 1990 1994) compared to the younger roofs (3 4 years old; installed 1998 1999).
In the first case, soil stiffness are varied from (E_{s}) = 0.8 to 1, 2, 4 and 8 MPa while the granular piles stiffness, (E_{gp}), remain constant as 40 MPa.
In the latter case, soil hydrophobicity resulting from heat effects creates patterns of variable wettability near the soil surface, where the burned areas can generate as much runoff as a paved surface, while the functional connectivity of unburned areas along the hillslope gradient has a large effect on runoff generation, reinfiltration, and propagation of concentrated flow (Moody et al., 2016).
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In some cases soil is a primary factor in inducing development of scrubland vegetation.
However, in these cases, soil P availability was distinctly higher and P CAL ranged between 35 and 45 mg/kg.
Due to their close soil characteristics, we hypothesized that in both cases, soil functioning is similar with respect to soil fauna activity.
In some cases, soil properties interacted with vegetation structure: soils high in clay content maintained high recruitment even with a decrease in production.
Except in a few cases, soil microbial respiration, biomass and activity were higher under zero tillage than under reduced tillage, both at planting and harvest sampling times.
The study shows that, in many cases, soil N2O emission peaks that were not predicted with the default model parameters were predicted after calibration.
The usual solution to this problem is to sample an equivalent mass (EM), but in most cases soil mass also changes over time.
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